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Mr. Ron Bottoms, City Manager <br />October 1, 2008 <br />Page 17 of 31 <br />k I o t z associates <br />Table 3 summarizes the type of studied channels for the first two above categories <br />(see also Exhibit 11). <br />Major drainage ditches or channels evaluated for the CWDS are of two types: 1) <br />those for which FEMA-based hydrologic and hydraulic models are available as a <br />basis for model creation, update and revision, and 2) those for which survey has <br />been done to approximately define the cross sectional shape of the channel. <br />The FEMA-based models are for extensive lengths of channel and for relatively <br />large drainage areas. The level of detail in the geometric description of these <br />models is good as evidenced by the number of cross sections used in the model <br />(see Exhibits 13, 14 and 15). Existing hydrologic and hydraulic models as given <br />by FEMA models for these major drainage ditches and channels were reviewed <br />and modified to reflect new conditions (e.g.,; change in channel. connectivity, <br />crossing structures, or land use) and information about the waterway and the <br />runoff to the waterway. These models provide a definitive description of flooding <br />conditions along the ditch or channel, and detailed conclusions about flow <br />containment or bank overflow along the length of the channel can be drawn. <br />On the other hand, those ditches and channels for which no prior hydrologic and <br />hydraulic models are available are generally short tributaries to the FEMA-based <br />models. Only limited data on ditch or channel geometry are available for these <br />ditches and channels; these data were obtained by field survey done for this study <br />(see Exhibits 13, 14, and 15). Typically only 2 or 3 cross sections were surveyed <br />along the ditch or channel. These survey data were collected for this study since <br />no existing data describing channel geometry for the tributaries were available. In <br />addition, information about structures (e.g., bridges) along the length of the <br />channel is generally incomplete. Consequently it is difficult to draw reliable <br />conclusions about the detailed behavior of water levels and consequent flow <br />containment within channel banks. (Along F101-00-00 for which a HEC-RAS <br />model was developed from hard copy data in the appendices of a master drainage <br />plan done by HCFCD for La Porte in 1987, two channel sections between Hwy <br />146 and Sens Road were field surveyed as a check on the cross section data in the <br />1987 master drainage plan study. Comparison of the survey cross section data to <br />the cross data provided in the 1987 showed the section data to be reasonable <br />consistent. Bank elevations and bank to bank distances were quite similar, as <br />were channel shape and side slopes except near the channel bottom. Flow line <br />elevations in the surveyed sections were about 4 ft deeper than the sections taken <br />from the 1987 study.) <br />